LEADER 01245nam0-22003971i-450- 001 990005497770203316 005 20021112120000.0 035 $a000549777 035 $aUSA01000549777 035 $a(ALEPH)000549777USA01 035 $a000549777 100 $a20010829d1994-------|0itac50------ba 101 $aita 102 $aIT 105 $a|||| ||||| 200 1 $aCorrespondence analysis in the social sciences$erecent developments and applications$fedited by Michael Greenacre, and Jorg Blasius 210 $aSan Diego$aLondon$cAcademic Press$d1994 215 $aXXI, 370 p.$d24 cm 606 $aScienze sociali$xMetodi di ricerca$2FI 620 $dLondon 620 $dSan Diego 676 $a300.1$cSuddivisioni standard$v21 702 1$aGREENACRE,$bMichael J. 702 1$aBLASIUS,$bJorg 712 $aAcademic press 801 $aIT$bSOL$c20120104 912 $a990005497770203316 950 $aDIP.TO SCIENZE ECONOMICHE - (SA)$dDS 300 300.1 GRE$e9755 DISES 951 $a300 300.1 GRE$b9755 DISES 959 $aBK 969 $aDISES 979 $c20121027$lUSA01$h1532 979 $c20121027$lUSA01$h1613 996 $aCorrespondence analysis in the social sciences$91129349 997 $aUNISA NUM $aUSA10493 LEADER 02161nam 2200529 450 001 9910786652903321 005 20200520144314.0 010 $a3-03826-461-X 035 $a(CKB)3710000000168241 035 $a(EBL)1910776 035 $a(SSID)ssj0001339888 035 $a(PQKBManifestationID)11758546 035 $a(PQKBTitleCode)TC0001339888 035 $a(PQKBWorkID)11352390 035 $a(PQKB)11607541 035 $a(MiAaPQ)EBC1910776 035 $a(Au-PeEL)EBL1910776 035 $a(CaPaEBR)ebr10895059 035 $a(OCoLC)884802403 035 $a(EXLCZ)993710000000168241 100 $a20140721h20142014 uy 0 101 0 $aeng 135 $aur|n|---||||| 181 $ctxt 182 $cc 183 $acr 200 00$aDiffusion and conduction in zeolites $edata compilation /$fedited by D. J. Fisher 210 1$a[Zurich, Switzerland] :$cTrans Tech Publications,$d[2014] 210 4$dİ[2014] 215 $a1 online resource (169 p.) 225 1 $aDefect and Diffusion Forum ;$vv.351 300 $aDescription based upon print version of record. 311 $a3-03835-080-X 327 $aDiffusion and Conduction in Zeolites; Table of Contents; Abstracts 330 $aThe microporous aluminosilicate minerals known as Zeolites are invaluable as adsorbents, molecular sieves and catalysts because they possess a porous structure that can let pass or accommodate cations such as, Ca2+, K+, Mg2+, Na+, etc. These are nevertheless loosely held and can be easily exchanged for those in an adjacent solution. Movement of other materials through Zeolites is naturally an important factor. The present compilation consists of diffusion data. These represent, as far as possible, pure diffusion, shorn of other transfer mechanisms such as permeation. Most of the results involv 410 0$aDefect and Diffusion Forum 606 $aZeolites 615 0$aZeolites. 676 $a660.2995 702 $aFisher$b D. J. 801 0$bMiAaPQ 801 1$bMiAaPQ 801 2$bMiAaPQ 906 $aBOOK 912 $a9910786652903321 996 $aDiffusion and conduction in zeolites$93818897 997 $aUNINA